Rhobell Fawr

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Rhobell Fawr
Rhobell Fawr summit.JPG
The summit of Rhobell Fawr
Highest point
Elevation 734 m (2,408 ft)
Prominence 309 m (1,014 ft)
Parent peak Arenig Fawr
Listing Marilyn, Hewitt, Nuttall
Coordinates 52°48′50″N3°48′07″W / 52.814°N 3.802°W / 52.814; -3.802 Coordinates: 52°48′50″N3°48′07″W / 52.814°N 3.802°W / 52.814; -3.802
Naming
PronunciationWelsh:  [ˈr̥ɔbɛɬ ˈvaur]
Geography
Location Gwynedd, Wales
Parent range Snowdonia
OS grid SH786256
Topo map OS Landranger 124
Listed summits of Rhobell Fawr
NameGrid refHeightStatus
Dduallt 662 m (2,172 ft) Hewitt, Nuttall
Rhobell Ganol521 m (1,709 ft) TuMP
Rhobell-y-big504 m (1,654 ft) Dodd (hill), Dewey (hill)

Rhobell Fawr is the site of an ancient volcano that was active during the Early Ordovician period [1] [2] in the Arenig range within the Snowdonia National Park.

Despite its modest height of 734 m (2,408 feet), it is a mountain with views of higher peaks all around, including the north face of Cadair Idris and distant Snowdon.

The paths are not well trodden, but there is a distinct path up from Bwlch Goriwared, a couple of miles north-north-east of the small village of Llanfachreth.

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Glyderau

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Arenig Fawr

Arenig Fawr is a mountain in Snowdonia, North Wales, close to Llyn Celyn reservoir, alongside the A4212 between Trawsfynydd and Bala.

Dduallt

Dduallt is a mountain in central Snowdonia, north Wales. It is the sister peak of Rhobell Fawr.

Cwm Idwal

Cwm Idwal is a cirque in the Glyderau range of mountains in northern Snowdonia, the national park in the mountainous region of North Wales. Its main interest is to hill walkers and rock climbers, but it is also of interest to geologists and naturalists, given its combination of altitude, aspect (north-facing) and terrain. In a 2005 poll conducted by Radio Times, Cwm Idwal was ranked the 7th greatest natural wonder in Britain.

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Aran Benllyn

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Gau Graig

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Carnedd y Filiast (Cerrigydrudion)

Carnedd y Filiast is a mountain near Cerrigydrudion on the border of the Snowdonia National Park, North Wales and is 669 metres (2,195 ft) high.

Moel Llyfnant

Moel Llyfnant is a mountain in the southern portion of the Snowdonia National Park in Gwynedd, Wales. It is a peak in the Arenig mountain range. It lies to the west of Arenig Fawr. It has one notable top, the twin peaked Gallt y Daren, being at the end of its west ridge.

Yr Arddu (South)

Yr Arddu is a large hill in Snowdonia, Wales. It lies approximately 2.5 km south east of the village of Beddgelert and just over 1 km from the rather more famous mountain Cnicht. It is a rugged hill with widespread rock outcrops and cliffs. A small lake, Llyn yr Arddu, is located on the flanks of the mountain. The recognised summit is at 388m to the South of the hill, but the highest point, named Cerrig-y-Myllt on only the most detailed UK Ordnance Survey mapping, is at 463m above the two small lakes to the North of the hill. The craggy nature of the hill is due to the presence of lavas and tuffs dating from the Ordovician period when Snowdonia was characterised by numerous volcanic eruptions; Yr Arddu is a particularly good location to see the record of Ordovician volcanism. The Yr Arddu Tuffs may be the earliest eruptive phase of the Lower Rhyolitic Tuff Formation.

Fforest Fawr Geopark is a Geopark in the Brecon Beacons National Park, south Wales. It is the first designated Geopark in Wales having gained membership of both the European Geoparks Network and the UNESCO-assisted Global Network of National Geoparks in October 2005. The Geopark aims to promote and support sustainable tourism and other opportunities to improve the economy of the area whilst safeguarding the natural environment. Its aims largely coincide with the statutory duties and purpose of the National Park within which it sits.

Snowdon Volcanic Group

The Snowdon Volcanic Group is an Ordovician lithostratigraphic group in Snowdonia, north-west Wales. The name is derived from Snowdon, the highest peak in Wales where it outcrops. This assemblage of rocks has also been referred to as the Snowdon Volcanic Series.

Pen Ty-Nant

Pen Ty-Nant is a hill within the Snowdonia National Park in Gwynedd, North Wales.

The geology of Snowdonia National Park is dominated by sedimentary and volcanic rocks from the Cambrian and Ordovician periods with intrusions of Ordovician and Silurian age. There are Silurian and Cenozoic sedimentary rocks on the park's margins. The succession was intensely faulted and folded during the Caledonian Orogeny. The region was uplifted as the North Atlantic Ocean opened during the Cenozoic. The current mountainous landscape arises from repeated glaciations during the Quaternary period.

References

  1. Geoscience Wales (2015). "Rhobell Fawr: The First Signs of Ordovician Volcanism in North Wales".
  2. "North West Wales Outdoors: Snowdon". BBC. 2002. Archived from the original on 16 October 2006.